Hydromorphological processes of Dongting Lake in China between 1951 and 2014

Under the impact of intensive anthropogenic activities and in the context of global climate change, the hydromorphological processes of most lakes around the world have changed dramatically. Here, based on hydrologic and topographic data, we analyzed secular variations in hydromorphological characteristics and their influencing factors at Dongting Lake, the second-largest freshwater lake in China. The entire time series (1951–2014) was divided into four subperiods based on the anthropogenic modifications of the Changjiang (Yangtze) River, including the construction of the Lower Jingjiang Cutoff Project and the operation of the Gezhou Dam (GD) and the Three Gorges Dam (TGD). The results indicated that there were obvious stepwise decreasing trends in the annual water discharge and suspended sediment discharge (SSD) from 1951 to 2014. Seasonal differences in water discharge and SSD over the recent 60 years exhibited a tendency of “less flooding during the flood season and more drying during the dry season”. Meanwhile, the deposition-erosion budget of Dongting Lake shifted from a deposition rate of 120 × 10⁶ t/yr from 1951 to 2003 to an erosion rate of 2 × 10⁶ t/yr with the serious degradation of the Ouchi and Xiangjiang deltas after 2003. The hydrological processes of Dongting Lake are dominated by different anthropogenic activities at different stages. The Jingjiang Cutoff Project is the main driver of the decreases in water discharge and SSD from 1967 to 1980. The operation of the GD along the Changjiang River and other reservoirs, as well as land-use changes in the Dongting Lake basin, should be responsible for the hydrological variations from 1981 to 2003. The high sediment retention rate, geometric adjustment of the channel, and flow regulation induced by the operation of the TGD are the main drivers for the hydromorphological variations in Dongting Lake in 2004–2014.